Frolov yuri (34 risultati)
Lingua: Inglese
Editore: Novosti Press Agency Publishing House, Moscow, 1986
- Brossura
- Manoscritto
Da: The People's Co-op Bookstore, Vancouver, BC, CanadaThe People's Co-op Bookstore
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EUR 10,27
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Soft cover. Condizione: Near Fine. 5" x 7-7/8", 24pp. Saddle stitched pamphlet in printed card stock cover. Some edge wear to the spine, and the bottom inside corner is a bit bent/creased. Original bookseller's price sticker still affixed to back cover. Binding remains sound; staples are free of rust. Pages are clean and bright…and unmarked.
Editore: USGS, 2005
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Da: Crossroads Books, Reno, NV, U.S.A.Crossroads Books
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Condizione: Nuovo
EUR 36,92
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Condizione: new. "The Proterozoic and Phanerozoic metallogenic and tectonic evolution of the Russian Far East, Alaska, and the Canadian Cordillera is recorded in the cratons, craton margins, and orogenic collages of the Circum-North Pacific mountain belts that separate the North Pacific from the eastern North Asian and western N…orth American Cratons. The collages consist of tectonostratigraphic terranes and contained metallogenic belts, which are composed of fragments of igneous arcs, accretionary-wedge and subduction-zone complexes, passive continental margins, and cratons. The terranes are overlapped by continental-margin-arc and sedimentary-basin assemblages and contained metallogenic belts. The metallogenic and geologic history of terranes, overlap assemblages, cratons, and craton margins has been complicated by postaccretion dismemberment and translation during strike-slip faulting that occurred subparallel to continental margins. Seven processes overlapping in time were responsible for most of metallogenic and geologic complexities of the region (1) In the Early and Middle Proterozoic, marine sedimentary basins developed on major cratons and were the loci for ironstone (Superior Fe) deposits and sediment-hosted Cu deposits that occur along both the North Asia Craton and North American Craton Margin. (2) In the Late Proterozoic, Late Devonian, and Early Carboniferous, major periods of rifting occurred along the ancestral margins of present-day Northeast Asia and northwestern North America. The rifting resulted in fragmentation of each continent, and formation of cratonal and passive continental-margin terranes that eventually migrated and accreted to other sites along the evolving margins of the original or adjacent continents. The rifting also resulted in formation of various massive-sulfide metallogenic belts. (3) From about the late Paleozoic through the mid-Cretaceous, a succession of island arcs and contained igneous-arc-related metallogenic belts and tectonically paired subduction zones formed near continental margins. (4) From about mainly the mid-Cretaceous through the present, a succession of continental-margin igneous arcs (some extending offshore into island arcs) and contained metallogenic belts, and tectonically paired subduction zones formed along the continental margins. (5) From about the Jurassic to the present, oblique convergence and rotations caused orogen-parallel sinistral, and then dextral displacements within the plate margins of the Northeast Asian and North American Cratons. The oblique convergences and rotations resulted in the fragmentation, displacement, and duplication of formerly more continuous arcs, subduction zones, passive continental margins, and contained metallogenic belts. These fragments were subsequently accreted along the margins of the expanding continental margins. (6) From the Early Jurassic through Tertiary, movement of the upper continental plates toward subduction zones resulted in strong plate coupling and accretion of the former island arcs, subduction zones, and contained metallogenic belts to continental margins. In this region, the multiple arc accretions were accompanied and followed by crustal thickening, anatexis, metamorphism, formation of collision-related metallogenic belts, and uplift; this resulted in the substantial growth of the North Asian and North American continents. (7) In the middle and late Cenozoic, oblique to orthogonal convergence of the Pacific Plate with present-day Alaska and Northeast Asia resulted in formation of the present ring of volcanoes and contained metallogenic belts around the Circum-North Pacific. Oblique convergence between the Pacific Plate and Alaska also resulted in major dextral-slip faulting in interior and southern Alaska and along the western part of the Aleutian- Wrangell arc. Associated with dextral-slip faulting was crustal extrusion of terranes from western Alaska into the Bering Sea. " DV2. softcover, wrapped in shrink wrap, tight, crisp, 429 pages.
Editore: USGS, 2005
- Brossura
Da: Crossroads Books, Reno, NV, U.S.A.Crossroads Books
Contatta il venditoreVenditore con 5 stelleMembro dell’associazione: IOBA
Condizione: Nuovo
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Condizione: new. "The Proterozoic and Phanerozoic metallogenic and tectonic evolution of the Russian Far East, Alaska, and the Canadian Cordillera is recorded in the cratons, craton margins, and orogenic collages of the Circum-North Pacific mountain belts that separate the North Pacific from the eastern North Asian and western N…orth American Cratons. The collages consist of tectonostratigraphic terranes and contained metallogenic belts, which are composed of fragments of igneous arcs, accretionary-wedge and subduction-zone complexes, passive continental margins, and cratons. The terranes are overlapped by continental-margin-arc and sedimentary-basin assemblages and contained metallogenic belts. The metallogenic and geologic history of terranes, overlap assemblages, cratons, and craton margins has been complicated by postaccretion dismemberment and translation during strike-slip faulting that occurred subparallel to continental margins. Seven processes overlapping in time were responsible for most of metallogenic and geologic complexities of the region (1) In the Early and Middle Proterozoic, marine sedimentary basins developed on major cratons and were the loci for ironstone (Superior Fe) deposits and sediment-hosted Cu deposits that occur along both the North Asia Craton and North American Craton Margin. (2) In the Late Proterozoic, Late Devonian, and Early Carboniferous, major periods of rifting occurred along the ancestral margins of present-day Northeast Asia and northwestern North America. The rifting resulted in fragmentation of each continent, and formation of cratonal and passive continental-margin terranes that eventually migrated and accreted to other sites along the evolving margins of the original or adjacent continents. The rifting also resulted in formation of various massive-sulfide metallogenic belts. (3) From about the late Paleozoic through the mid-Cretaceous, a succession of island arcs and contained igneous-arc-related metallogenic belts and tectonically paired subduction zones formed near continental margins. (4) From about mainly the mid-Cretaceous through the present, a succession of continental-margin igneous arcs (some extending offshore into island arcs) and contained metallogenic belts, and tectonically paired subduction zones formed along the continental margins. (5) From about the Jurassic to the present, oblique convergence and rotations caused orogen-parallel sinistral, and then dextral displacements within the plate margins of the Northeast Asian and North American Cratons. The oblique convergences and rotations resulted in the fragmentation, displacement, and duplication of formerly more continuous arcs, subduction zones, passive continental margins, and contained metallogenic belts. These fragments were subsequently accreted along the margins of the expanding continental margins. (6) From the Early Jurassic through Tertiary, movement of the upper continental plates toward subduction zones resulted in strong plate coupling and accretion of the former island arcs, subduction zones, and contained metallogenic belts to continental margins. In this region, the multiple arc accretions were accompanied and followed by crustal thickening, anatexis, metamorphism, formation of collision-related metallogenic belts, and uplift; this resulted in the substantial growth of the North Asian and North American continents. (7) In the middle and late Cenozoic, oblique to orthogonal convergence of the Pacific Plate with present-day Alaska and Northeast Asia resulted in formation of the present ring of volcanoes and contained metallogenic belts around the Circum-North Pacific. Oblique convergence between the Pacific Plate and Alaska also resulted in major dextral-slip faulting in interior and southern Alaska and along the western part of the Aleutian- Wrangell arc. Associated with dextral-slip faulting was crustal extrusion of terranes from western Alaska into the Bering Sea. " DV1. softcover, wrapped in shrink wrap, tight, crisp, 429 pages.
Editore: USGS, 2005
- Brossura
Da: Crossroads Books, Reno, NV, U.S.A.Crossroads Books
Contatta il venditoreVenditore con 5 stelleMembro dell’associazione: IOBA
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Condizione: new. "The Proterozoic and Phanerozoic metallogenic and tectonic evolution of the Russian Far East, Alaska, and the Canadian Cordillera is recorded in the cratons, craton margins, and orogenic collages of the Circum-North Pacific mountain belts that separate the North Pacific from the eastern North Asian and western N…orth American Cratons. The collages consist of tectonostratigraphic terranes and contained metallogenic belts, which are composed of fragments of igneous arcs, accretionary-wedge and subduction-zone complexes, passive continental margins, and cratons. The terranes are overlapped by continental-margin-arc and sedimentary-basin assemblages and contained metallogenic belts. The metallogenic and geologic history of terranes, overlap assemblages, cratons, and craton margins has been complicated by postaccretion dismemberment and translation during strike-slip faulting that occurred subparallel to continental margins. Seven processes overlapping in time were responsible for most of metallogenic and geologic complexities of the region (1) In the Early and Middle Proterozoic, marine sedimentary basins developed on major cratons and were the loci for ironstone (Superior Fe) deposits and sediment-hosted Cu deposits that occur along both the North Asia Craton and North American Craton Margin. (2) In the Late Proterozoic, Late Devonian, and Early Carboniferous, major periods of rifting occurred along the ancestral margins of present-day Northeast Asia and northwestern North America. The rifting resulted in fragmentation of each continent, and formation of cratonal and passive continental-margin terranes that eventually migrated and accreted to other sites along the evolving margins of the original or adjacent continents. The rifting also resulted in formation of various massive-sulfide metallogenic belts. (3) From about the late Paleozoic through the mid-Cretaceous, a succession of island arcs and contained igneous-arc-related metallogenic belts and tectonically paired subduction zones formed near continental margins. (4) From about mainly the mid-Cretaceous through the present, a succession of continental-margin igneous arcs (some extending offshore into island arcs) and contained metallogenic belts, and tectonically paired subduction zones formed along the continental margins. (5) From about the Jurassic to the present, oblique convergence and rotations caused orogen-parallel sinistral, and then dextral displacements within the plate margins of the Northeast Asian and North American Cratons. The oblique convergences and rotations resulted in the fragmentation, displacement, and duplication of formerly more continuous arcs, subduction zones, passive continental margins, and contained metallogenic belts. These fragments were subsequently accreted along the margins of the expanding continental margins. (6) From the Early Jurassic through Tertiary, movement of the upper continental plates toward subduction zones resulted in strong plate coupling and accretion of the former island arcs, subduction zones, and contained metallogenic belts to continental margins. In this region, the multiple arc accretions were accompanied and followed by crustal thickening, anatexis, metamorphism, formation of collision-related metallogenic belts, and uplift; this resulted in the substantial growth of the North Asian and North American continents. (7) In the middle and late Cenozoic, oblique to orthogonal convergence of the Pacific Plate with present-day Alaska and Northeast Asia resulted in formation of the present ring of volcanoes and contained metallogenic belts around the Circum-North Pacific. Oblique convergence between the Pacific Plate and Alaska also resulted in major dextral-slip faulting in interior and southern Alaska and along the western part of the Aleutian- Wrangell arc. Associated with dextral-slip faulting was crustal extrusion of terranes from western Alaska into the Bering Sea." DV4. softcover, wrapped in shrink wrap, tight, crisp, 429 pages.
Editore: USGS, 2005
- Brossura
Da: Crossroads Books, Reno, NV, U.S.A.Crossroads Books
Contatta il venditoreVenditore con 5 stelleMembro dell’associazione: IOBA
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Condizione: new. The Proterozoic and Phanerozoic metallogenic and tectonic evolution of the Russian Far East, Alaska, and the Canadian Cordillera is recorded in the cratons, craton margins, and orogenic collages of the Circum-North Pacific mountain belts that separate the North Pacific from the eastern North Asian and western No…rth American Cratons. The collages consist of tectonostratigraphic terranes and contained metallogenic belts, which are composed of fragments of igneous arcs, accretionary-wedge and subduction-zone complexes, passive continental margins, and cratons. The terranes are overlapped by continental-margin-arc and sedimentary-basin assemblages and contained metallogenic belts. The metallogenic and geologic history of terranes, overlap assemblages, cratons, and craton margins has been complicated by postaccretion dismemberment and translation during strike-slip faulting that occurred subparallel to continental margins. Seven processes overlapping in time were responsible for most of metallogenic and geologic complexities of the region (1) In the Early and Middle Proterozoic, marine sedimentary basins developed on major cratons and were the loci for ironstone (Superior Fe) deposits and sediment-hosted Cu deposits that occur along both the North Asia Craton and North American Craton Margin. (2) In the Late Proterozoic, Late Devonian, and Early Carboniferous, major periods of rifting occurred along the ancestral margins of present-day Northeast Asia and northwestern North America. The rifting resulted in fragmentation of each continent, and formation of cratonal and passive continental-margin terranes that eventually migrated and accreted to other sites along the evolving margins of the original or adjacent continents. The rifting also resulted in formation of various massive-sulfide metallogenic belts. (3) From about the late Paleozoic through the mid-Cretaceous, a succession of island arcs and contained igneous-arc-related metallogenic belts and tectonically paired subduction zones formed near continental margins. (4) From about mainly the mid-Cretaceous through the present, a succession of continental-margin igneous arcs (some extending offshore into island arcs) and contained metallogenic belts, and tectonically paired subduction zones formed along the continental margins. (5) From about the Jurassic to the present, oblique convergence and rotations caused orogen-parallel sinistral, and then dextral displacements within the plate margins of the Northeast Asian and North American Cratons. The oblique convergences and rotations resulted in the fragmentation, displacement, and duplication of formerly more continuous arcs, subduction zones, passive continental margins, and contained metallogenic belts. These fragments were subsequently accreted along the margins of the expanding continental margins. (6) From the Early Jurassic through Tertiary, movement of the upper continental plates toward subduction zones resulted in strong plate coupling and accretion of the former island arcs, subduction zones, and contained metallogenic belts to continental margins. In this region, the multiple arc accretions were accompanied and followed by crustal thickening, anatexis, metamorphism, formation of collision-related metallogenic belts, and uplift; this resulted in the substantial growth of the North Asian and North American continents. (7) In the middle and late Cenozoic, oblique to orthogonal convergence of the Pacific Plate with present-day Alaska and Northeast Asia resulted in formation of the present ring of volcanoes and contained metallogenic belts around the Circum-North Pacific. Oblique convergence between the Pacific Plate and Alaska also resulted in major dextral-slip faulting in interior and southern Alaska and along the western part of the Aleutian- Wrangell arc. Associated with dextral-slip faulting was crustal extrusion of terranes from western Alaska into the Bering Sea. DX1. softcover, wrapped in shrink wrap, tight, crisp, 429 pages.
Editore: USGS, 2005
- Brossura
Da: Crossroads Books, Reno, NV, U.S.A.Crossroads Books
Contatta il venditoreVenditore con 5 stelleMembro dell’associazione: IOBA
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Condizione: new. The Proterozoic and Phanerozoic metallogenic and tectonic evolution of the Russian Far East, Alaska, and the Canadian Cordillera is recorded in the cratons, craton margins, and orogenic collages of the Circum-North Pacific mountain belts that separate the North Pacific from the eastern North Asian and western No…rth American Cratons. The collages consist of tectonostratigraphic terranes and contained metallogenic belts, which are composed of fragments of igneous arcs, accretionary-wedge and subduction-zone complexes, passive continental margins, and cratons. The terranes are overlapped by continental-margin-arc and sedimentary-basin assemblages and contained metallogenic belts. The metallogenic and geologic history of terranes, overlap assemblages, cratons, and craton margins has been complicated by postaccretion dismemberment and translation during strike-slip faulting that occurred subparallel to continental margins. Seven processes overlapping in time were responsible for most of metallogenic and geologic complexities of the region (1) In the Early and Middle Proterozoic, marine sedimentary basins developed on major cratons and were the loci for ironstone (Superior Fe) deposits and sediment-hosted Cu deposits that occur along both the North Asia Craton and North American Craton Margin. (2) In the Late Proterozoic, Late Devonian, and Early Carboniferous, major periods of rifting occurred along the ancestral margins of present-day Northeast Asia and northwestern North America. The rifting resulted in fragmentation of each continent, and formation of cratonal and passive continental-margin terranes that eventually migrated and accreted to other sites along the evolving margins of the original or adjacent continents. The rifting also resulted in formation of various massive-sulfide metallogenic belts. (3) From about the late Paleozoic through the mid-Cretaceous, a succession of island arcs and contained igneous-arc-related metallogenic belts and tectonically paired subduction zones formed near continental margins. (4) From about mainly the mid-Cretaceous through the present, a succession of continental-margin igneous arcs (some extending offshore into island arcs) and contained metallogenic belts, and tectonically paired subduction zones formed along the continental margins. (5) From about the Jurassic to the present, oblique convergence and rotations caused orogen-parallel sinistral, and then dextral displacements within the plate margins of the Northeast Asian and North American Cratons. The oblique convergences and rotations resulted in the fragmentation, displacement, and duplication of formerly more continuous arcs, subduction zones, passive continental margins, and contained metallogenic belts. These fragments were subsequently accreted along the margins of the expanding continental margins. (6) From the Early Jurassic through Tertiary, movement of the upper continental plates toward subduction zones resulted in strong plate coupling and accretion of the former island arcs, subduction zones, and contained metallogenic belts to continental margins. In this region, the multiple arc accretions were accompanied and followed by crustal thickening, anatexis, metamorphism, formation of collision-related metallogenic belts, and uplift; this resulted in the substantial growth of the North Asian and North American continents. (7) In the middle and late Cenozoic, oblique to orthogonal convergence of the Pacific Plate with present-day Alaska and Northeast Asia resulted in formation of the present ring of volcanoes and contained metallogenic belts around the Circum-North Pacific. Oblique convergence between the Pacific Plate and Alaska also resulted in major dextral-slip faulting in interior and southern Alaska and along the western part of the Aleutian- Wrangell arc. Associated with dextral-slip faulting was crustal extrusion of terranes from western Alaska into the Bering Sea. softcover, wrapped in shrink wrap, tight, crisp, 429 pages.
Work and the Brain : Pavlov's Teaching and Its Application to Problems of Scientific Organisation of Work
Frolov, Yuri (Translated by Xenia Danko. Edited by David Myshne)
Editore: Foreign Languages Publishing House, Moscow, 1963
- Rilegato
Da: Harropian Books, IOBA, Nelson, BC, CanadaHarropian Books, IOBA
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Condizione: Usato - Molto buono
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Hardcover. Condizione: Very Good. Condizione sovraccoperta: Very Good. Light blue cloth over boards, title and decorations stamped in blue onto top board and spine, small 8vo 7-3/4 inches tall, pp. 229, [230], illustrated with line drawings throughout. Volume with light fade to spine and top edge, endpapers toned. DJ with light…edge wear and soil. ".one of the first Soviet popular-science publications in the field of biology. " from the Preface.
Editore: Editorial Platina, 1965
- Brossura
Da: LibroUsado | TikBooks, Madrid, M, SpagnaLibroUsado | TikBooks
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Encuadernación de tapa blanda. Condizione: Regular. L705433. Editorial Platina - 182pp (H) Muy amarillento por el paso del tiempo. Corte de las hojas no uniforme en el corte superior. Ro.
Magnetic Resonance And Its Applications
Chizhik, Vladimir I.; Chernyshev, Yuri S.; Donets, Alexey V.; Frolov, Vyacheslav V.; Komolkin, Andrei V.; Shelyapina, Marina G.
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Da: Romtrade Corp., STERLING HEIGHTS, MI, U.S.A.Romtrade Corp.
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Spedizione gratuitaSpedito in U.S.A.Quantità: 1 disponibili
Condizione: New. This is a Brand-new US Edition. This Item may be shipped from US or any other country as we have multiple locations worldwide.
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Da: GreatBookPrices, Columbia, MD, U.S.A.GreatBookPrices
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Condizione: New.
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Da: California Books, Miami, FL, U.S.A.California Books
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Condizione: New.
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Condizione: As New. Unread book in perfect condition.
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Da: Ria Christie Collections, Uxbridge, Regno UnitoRia Christie Collections
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Condizione: New. In.
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Da: Majestic Books, Hounslow, Regno UnitoMajestic Books
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Condizione: New.
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Condizione: New. 1st edition NO-PA16APR2015-KAP.
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Da: Biblios, frankfurt am main, HESSE, GermaniaBiblios
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Condizione: New.
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Hardcover. Condizione: Brand New. 118 pages. 8.50x5.43x8.74 inches. In Stock.
Magnetic Resonance and Its Applications
Chizhik, Vladimir I. I.; Chernyshev, Yuri S.; Donets, Alexey V.; Frolov, Vyacheslav V.; Komolkin, Andrei V.; Shelyapina, Marina G.
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Da: Books Puddle, New York, NY, U.S.A.Books Puddle
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Condizione: New. pp. 782.
Magnetic Resonance and Its Applications
Chizhik, Vladimir I./ Chernyshev, Yuri S./ Donets, Alexey V./ Frolov, Viatcheslav/ Komolkin, Andrei
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Da: Revaluation Books, Exeter, Regno UnitoRevaluation Books
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Paperback. Condizione: Brand New. reprint edition. 804 pages. 9.25x6.10x1.82 inches. In Stock.
Da: Náufragos, Sant Just Desvern, B, SpagnaNáufragos
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Editorial Platina,Col.El Ser y la Conciencia,Buenos Aires 1965.20 cm.182 pag.Enc.rústica Editorial .En buen estado,con alguna anotación marginal del anterior poseedor en 3 de las primeras páginas sin afectar al texto. Relaciones entre el sistema nervioso y el trabajo mental,y de éste con el trabajo físico.
Editore: Voronezh, 1980
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Da: BiblioEra, Everett, MA, U.S.A.BiblioEra
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Hardcover. Condizione: Good. In Russian. Frolov, Yuri Mikhailovich. A summary of lectures on the Electrodrive course. Voronezh: VPI, All images are for identification of editions only. Several books of the same edition may be available. Please feel free to request photos of available books.SKU1016795.
Editore: Moscow, 1970
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Da: BiblioEra, Everett, MA, U.S.A.BiblioEra
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Hardcover. Condizione: Good. In Russian. Frolov, Yuri Nikolaevich. Elements of linear algebra. Moscow: 1970. All images are for identification of editions only. Several books of the same edition may be available. Please feel free to request photos of available books.SKU7066252.
Sovetskiy sud na strazhe prav grazhdan. In Russian /The Soviet Court on the Guard of Citizens Rights
Editore: Kyiv, 1976
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Da: BiblioEra, Everett, MA, U.S.A.BiblioEra
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Hardcover. Condizione: Good. In Russian. Frolov, Yuri Anisimovich. The Soviet Court on the Guard of Citizens Rights. Kyiv: 1976. All images are for identification of editions only. Several books of the same edition may be available. Please feel free to request photos of available books.SKU6955400.
Editore: Kyiv, 1970
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Da: BiblioEra, Everett, MA, U.S.A.BiblioEra
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EUR 179,19
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Hardcover. Condizione: Good. In Russian. Frolov, Yuri Anisimovich. Court and Prosecutor's Office of bourgeois states. Kyiv: 1970. All images are for identification of editions only. Several books of the same edition may be available. Please feel free to request photos of available books.SKU7066248.
Editore: Kyiv, 1971
- Rilegato
Da: BiblioEra, Everett, MA, U.S.A.BiblioEra
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EUR 179,19
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Hardcover. Condizione: Good. In Russian. Frolov, Yuri Anisimovich. The Soviet Judicial System. Kyiv: 1970 vol. 1971. All images are for identification of editions only. Several books of the same edition may be available. Please feel free to request photos of available books.SKU7066247.
Editore: Izhevsk, 1971
- Rilegato
Da: BiblioEra, Everett, MA, U.S.A.BiblioEra
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EUR 179,19
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Hardcover. Condizione: Good. In Russian. Frolov, Yuri Fedorovich. Poetry in the grass. Izhevsk: Udmurtia, 1971. All images are for identification of editions only. Several books of the same edition may be available. Please feel free to request photos of available books.SKU7066253.
Magnetic Resonance and Its Applications
Chizhik, Vladimir I.; Chernyshev, Yuri S.; Donets, Alexey V.; Frolov, Vyacheslav V.; Komolkin, Andrei V.; Shelyapina, Marina G.
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Da: Basi6 International, Irving, TX, U.S.A.Basi6 International
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Condizione: Brand New. New. US edition. Print on demand title. Delivery takes 20-25 days.
Limit States of Compressed Concrete Elements by Transverse Deformations
Iakov Iskhakov (Ariel University, Israel)|Ilya Frolov|Yuri Ribakov (Ariel University, Israel)
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Da: moluna, Greven, Germaniamoluna
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Condizione: New. Dieser Artikel ist ein Print on Demand Artikel und wird nach Ihrer Bestellung fuer Sie gedruckt. Iakov Iskhakov is a Full Professor at Ariel University, Israel. The main scientific activity is focused on reinforced concrete structures and seismic resistance. He has published 14 books, more than 120 papers in sci…entific journals and presented .
